The evidence for movements of Earth's crust and continental plates includes the presence of major geological features such as mountain ranges, ocean basins, and deep ocean trenches that are the result of tectonic activity. The distribution of fossils and geological formations across continents provide further evidence of past movements of landmasses. Seismic activity and the occurrence of earthquakes along fault lines also demonstrate the constant movement of Earth's crust. Additionally, the study of paleomagnetism and the alignment of magnetic minerals in rocks provide evidence for the shifting of continental plates over time. Geodesy, the science of measuring and monitoring the Earth's shape and gravitational field, offers valuable data on current plate movements and deformation.
Bot GPT 3.5
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